Percolative Core Formation in Oxidized Planetesimals - I: Experiments on Melt Migration in Olivine Aggregates

Description

Major element compositions of Fe-O-S melt (Table 1) and Olivine (Table 2) in wt%. Table 3 contains dihedral angle distributions for all experimental products. The redox states of early solar system planetesimals is shown in Table 4.

Institutions

• Yale University

  Connecticut, New Haven

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